Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean
The deglacial delta C-13 minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad delta C-13 minimum event was also reported as far...
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/32931 2023-05-15T13:40:37+02:00 Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean Chen ShuangXi Li TieGang Tang Zheng Qiu XiaoHua Xiong ZhiFang Nan QingYun Xu ZhaoKai Chang FengMing 2011-08-01 http://ir.qdio.ac.cn/handle/337002/32931 https://doi.org/10.1007/s11434-011-4590-0 英语 eng CHINESE SCIENCE BULLETIN http://ir.qdio.ac.cn/handle/337002/32931 doi:10.1007/s11434-011-4590-0 Planktonic Foraminiferal Delta C-13 Ventilation Of The Deep souThern Ocean Northwestern Pacific Last Deglaciation Delta C-13 Minimum Event Article 期刊论文 2011 ftchinacasciocas https://doi.org/10.1007/s11434-011-4590-0 2022-06-27T05:37:11Z The deglacial delta C-13 minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad delta C-13 minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of influence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS(14)C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in delta C-13 records of both surface (Globigerinoides ruber) and subsurface (Pulleniatina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the delta C-13 record of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad delta C-13 minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low delta C-13 signal was transmitted. Subsurface water primarily received the low delta C-13 signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Southern Ocean Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Antarctic Pacific Southern Ocean The Antarctic Chinese Science Bulletin 56 24 2628 2634 |
institution |
Open Polar |
collection |
Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
op_collection_id |
ftchinacasciocas |
language |
English |
topic |
Planktonic Foraminiferal Delta C-13 Ventilation Of The Deep souThern Ocean Northwestern Pacific Last Deglaciation Delta C-13 Minimum Event |
spellingShingle |
Planktonic Foraminiferal Delta C-13 Ventilation Of The Deep souThern Ocean Northwestern Pacific Last Deglaciation Delta C-13 Minimum Event Chen ShuangXi Li TieGang Tang Zheng Qiu XiaoHua Xiong ZhiFang Nan QingYun Xu ZhaoKai Chang FengMing Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean |
topic_facet |
Planktonic Foraminiferal Delta C-13 Ventilation Of The Deep souThern Ocean Northwestern Pacific Last Deglaciation Delta C-13 Minimum Event |
description |
The deglacial delta C-13 minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad delta C-13 minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of influence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS(14)C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in delta C-13 records of both surface (Globigerinoides ruber) and subsurface (Pulleniatina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the delta C-13 record of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad delta C-13 minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low delta C-13 signal was transmitted. Subsurface water primarily received the low delta C-13 signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The ... |
format |
Article in Journal/Newspaper |
author |
Chen ShuangXi Li TieGang Tang Zheng Qiu XiaoHua Xiong ZhiFang Nan QingYun Xu ZhaoKai Chang FengMing |
author_facet |
Chen ShuangXi Li TieGang Tang Zheng Qiu XiaoHua Xiong ZhiFang Nan QingYun Xu ZhaoKai Chang FengMing |
author_sort |
Chen ShuangXi |
title |
Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean |
title_short |
Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean |
title_full |
Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean |
title_fullStr |
Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean |
title_full_unstemmed |
Response of the northwestern Pacific upper water delta C-13 to the last deglacial ventilation of the deep Southern Ocean |
title_sort |
response of the northwestern pacific upper water delta c-13 to the last deglacial ventilation of the deep southern ocean |
publishDate |
2011 |
url |
http://ir.qdio.ac.cn/handle/337002/32931 https://doi.org/10.1007/s11434-011-4590-0 |
geographic |
Antarctic Pacific Southern Ocean The Antarctic |
geographic_facet |
Antarctic Pacific Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctica Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica Southern Ocean |
op_relation |
CHINESE SCIENCE BULLETIN http://ir.qdio.ac.cn/handle/337002/32931 doi:10.1007/s11434-011-4590-0 |
op_doi |
https://doi.org/10.1007/s11434-011-4590-0 |
container_title |
Chinese Science Bulletin |
container_volume |
56 |
container_issue |
24 |
container_start_page |
2628 |
op_container_end_page |
2634 |
_version_ |
1766137534433198080 |